地貌面、地文期与地貌演化——从华北地貌演化研究看地貌学的一些基本理论  

Geomorphology Surface,Physiographics Cycle and Geomorphology Evolution:Some Basic Theory on Geomorphology Inferred from Physiographics Evolvement in North China

作　　者：吴忱 

机构地区：[1]河北省地理科学研究所,河北石家庄050011

出　　处：《地理与地理信息科学》2008年第3期75-78,共4页Geography and Geo-Information Science

摘　　要：华北地貌的形成演化研究以传统地貌学理论戴维斯等的"地貌面"和"侵蚀旋回"理论为指导。研究表明,它基本适用于华北地貌的形成与演化;同时也发现了传统地貌学理论的不足。该文用华北地貌形成演化的实际资料弥补了这个不足,并进一步探讨了地貌形成演化理论的某些新观点。The study of geomorphology evolution is instructed by tradition physiognomy theory, the“geomorphology surface”and the“erosion cycle”, which was developed by W. M. Davis et al. It is proved by the geomorphology development and evolution in North China. However a few flaws on tradition physiognomy theory are found. In this paper, these flaws are recovered,and also some new view points about geomorphology development and evolution are discussed.

关 键 词：地貌面 地文期 地貌演化 

分 类 号：P931[天文地球—自然地理学]